用户名: 密码: 验证码:
中国煤炭资源分布特征与勘查开发前景研究
详细信息    本馆镜像全文|  推荐本文 |  |   获取CNKI官网全文
摘要
论述了主要含煤盆地和井字型构造格局的形成,在此基础上进行煤炭地质分区与勘查开发地质条件对比;通过煤炭资源与煤类分布图以及资源量统计论述了煤炭资源空间、数量和煤类分布特征;在构建勘查开发程度计算公式基础上对当前煤炭资源的勘查开发程度进行了定量分析,并结合煤炭资源的分布特征圈定了相应的潜力区块;通过煤炭资源产消的历史分析开展了对于未来煤炭资源的供需预测以及综合保障能力分析,最后指出煤炭资源勘查开发的发展趋势并提出初步建议。主要成果和认识如下:
     (1)含煤盆地经历了漫长的构造演化,形成了大陆区井字型构造格局,奠定了煤炭地质井型分区的基本格架;构造应力场性质分异是导致东西部主要含煤盆地的盆地类型、煤系宏观构造变形、勘查开发地质条件分异的根本控制因素;
     (2)太行以东断陷型含煤盆地面临巨厚新生界覆盖、断裂发育、高地温、高地压、高水压等问题,地质条件复杂;中西部坳陷型含煤盆地煤系埋藏浅,盆内变形微弱,地质条件简单,但水资源短缺、生态环境脆弱;就瓦斯而言多数矿井勘查开发条件差;
     (3)煤炭资源西多东少、北富南贫,而水资源东部多、西部少、南部多、北部少,山区多、平原少。煤炭资源与水资源、经济发展水平均呈明显逆向分布;各赋煤区煤炭资源的多寡与构造演化过程中作为长期稳定构造单元的古板块的分布及组成各赋煤区构造单元的多少具有某种对应关系,以华北、塔里木、扬子等大规模稳定古板块内部蕴含的煤炭资源量往往较大。
     (4)我国煤炭资源煤类齐全,从褐煤、低变质烟煤到无烟煤均有分布,但分布严重不均;
     (5)勘查开发程度定量分析表明:浅部勘查程度表现为东高西低、北高南低;开发程度表现为东高西低,南北分布特征不明显;蒙东、晋陕蒙宁、云贵川渝、北疆四分区以及神东、蒙东、晋北、晋中、陕北、新疆、云贵七大基地的资源前景无论在当前还是未来较长时期内均属较优之列;
     (6)未来煤炭资源产消均呈上凸式增长,2020年、2030年、2050年煤炭需求量分别为39亿吨、40亿吨和42亿吨左右,产能有能力与需求保持同步增长;煤炭进口量增加更有可能侧重于弥补某些特殊工业用途或优质煤炭资源的缺口上;总体上煤炭资源勘查开发保障能力较强。
     (7)未来东部地区勘查工作应侧重深部、大型推覆体之下以及老矿区外围煤炭地质精细勘查,同时注重煤层瓦斯与水文地质勘查工作;中西部在加强对于空白区和预测资源勘查力度的同时,加强对于保有尚未利用资源的勘查力度,提高勘探详查比例,形成资源梯级结构;
     (8)煤炭资源勘查开发在宏观和微观上均表现为战略西移,提出保护与减轻东部,稳定开发中部,加快开发西部的开发布局战略。
This study discusses the formation of coal bearing basins and well types tectonicframework, and on this basis compares the coal geological division with the geologicalconditions of exploration and development; discusses the characteristics of coal resourcesspace, quantity, and distribution though the distribution map of coal resources and coal types;does quantitative analysis for the exploration degree of present coal resources on the bases ofthe construction of exploration and development formula, and combines coal resourcedistribution characteristics delineates the potential block; predicts the coal resources supplyand demand in future and analyses the comprehensive support capability through thehistorical analysis of the production and consumption of coal resources, at last points out thedevelopment trend of the coal resources prospecting and offers initial proposals. The mainoutcomes and understanding are as follows:
     (1)Coal basin experienced tectonic evolution in long time, formed mainland area tectonicframework just like a well, and established the basic framework of coal geological well fontpartition. The differentiation of the tectonic stress field's nature is the fundamental factorswhich leaded to the differentiation of the major coal bearing basins in western and eastern,macroscopic structural deformation of coal measure and geological conditions of explorationand development.
     (2)Faulted coal basins to the east of Taihang mountain have some problems: thick Cenozoiccapping, fracture development, high ground temperature, high ground pressure, high waterpressure and so on; the coal series of depression type coal bearing basin in Midwest areshallow, within the basin, deformation is weak and geological conditions are simple, however,the water resource is lack and ecological environment is fragile; most mines' explorationconditions are poor in terms of gas;
     (3)Coal resources is rich in west and north, poor in east and south, however, the watersources is rich in east and south, poor in west and north, at the same time the water inmountain area is more than it in plain. Coal resources, water resources, and economicdevelopment are significantly reverse distribution.
     (4)China has various kinds of coal, for example lignite, Low metamorphic bituminous coal,anthracite and so on, but they have seriously uneven distribution.
     (5)The quantitative analysis of exploration and development degree shows: the explorationlevel in shallow part is high in east and north, low in west and south; and development level in west is higher than it in east, and the distribution characteristic is not obvious.Eastern InnerMogolia zone, Shanxi, Shaanxi, Inner Mongolia, Ningxia zone, Yunnan, Guizhou, Sichuan,Chongqing zone, and northern Xinjiang zone, eastern Shenmu base, Eastern Inner Mongoliabase, northern Shanxi base, central Shanxi base, northern Shaanxi base, Xinjiang base,Yunnan and Guizhou base all have superior prospect of resource no matter in current or in thefuture.
     (6)In the future, the production and sales of coal resources will increase. In2020,2030and2050, the coal demand respectively are3.9billion,4billion and4.2billion, and Capacity cankeep pace with the demand growth; Increase in coal imports are more likely to focus on fillingthe gaps of some special industrial use or high-quality coal resources.Support ability of coalresources prospecting and exploitation is strong.
     (7)The Future exploration work in the eastern region should focus on Deep,Under largenappe and coal geological exploration in the periphery of old mines,while focus on coalseam gas and hydrological geological prospecting work,strengthen the ownership of unusedexploration coal resource, improve the exploration survey proportion, forming resourcecascade structure.
     (8)Exploration and development of coal resource in the macro and micro are expressed as a"strategic shift".The paper proposed the development layout strategy as:"protection andalleviate the eastern zone,Steady development in the central zone,To speed up thedevelopment of the West zone"
引文
[1] Detlef van Vuuren,Zhou Fengqi,Bert de Vries. Energy and emission scenarios for China in the21stcentury-exploration of baseline development and mitigation options[J]. Energy Policy,2003,(31):369-387.
    [2] Eric D.Larson,Wu Zongxin,Pat DeLaquil. Future implications of China s energy-technologychoices[J]. Energy Policy,2003,(31):1189-1204.
    [3]Energy Information Administration L.S. Department of Energy International energy outlook2004「M」.Translated by Tsinghua Clear Energy Research and Education Center. Beijing: Tsinghua UniversityPress,2004:1-55.
    [4]Lan W H.Appfication of grey clustering method to atmospheric environmental assessment andcomparison with other methods[J].Arid Environmental Monitoring,1995,9(3):147-150.
    [5] Larsona E D,Wu Z,Delaquil P.Future implications of China’s energy-technology choices[J]. EncrgyPolicy,2003,31:1189-1204.
    [6] LIU H, Huang H, The Calculating Model for Development Investment of Coal Resources Based onANN. In5th International Symposium on Mining Science and Technology, XUZhou,2004.
    [7] Peter Nolan. China and the Global Economy:national champi ons,industrial policy,and the bigbusiness revolution [M].Houndmills,Basingstoke,Hampshire;New York Palgrave,2001.
    [8] Qi Ming, Rong Xilin, Tang Dazhang, et al. Petrographic and geochemical characterization of pale anddar k brown coal from Yunnan Province [J]. China Int J Coal Geol,1994,25(1):65-92.
    [9] Sellers E J,Klerck P.Modeling of the effect of discontinuities on the extent of the fracture zonesurrounding deep tunnels [J].Tunneling and Underground Space Technology,2000,15(4):463-469.
    [10]Zhou L, Xie L Q,Zhou L L, et al.Application ofgrey clustering method in eutrophication evaluationfor etland[J].Journal of Shenyang Agricultural University,2005,36(5):594-598.
    [11]张雷.矿产资源开发与国家工业化[M].北京:商务印书馆,2004.
    [12]李鑫,庄新国,周继兵等.准东煤田中部矿区西山窑组巨厚煤层煤相分析[J].地质科技情报.2010,29(5):84-88
    [13]漆家福,等.准噶尔盆地构造演化与重点区带构造变形机制研究(阶段报告)[M].石油大学,2005.
    [14]贾建称,张妙逢,龙亚平.中国含煤区地质背景与构造变形特征[J].安徽理工大学学报.2009,29(4):1-8
    [15]蔡忠贤,陈发景,贾振远.准噶尔盆地的类型和构造演化[J].地学前缘,2000,No416]新疆石油管理局勘探开发研究院.准噶尔盆地地震大剖面综合解释[M].新疆石油管理局,2000.
    [17]陈海泓,侯泉林,肖立交.中国碰撞造山带研究[M].海洋出版社,1999
    [18]郭华,李明,李守林,等.板内造山带主要构造特征研究[M].地质出版社,2002.
    [19]杨春志,等.吉林省松辽盆地东缘聚煤盆地的地质构造特征及聚煤规律研究[J].吉林地质.1987,1:1-7
    [20]吴克平,刘颖鑫,荆保沢,等.梅河盆地沉积聚煤环境与含煤远景[J].吉林地质.2008,3(27):24-29
    [21]王应林,等.内蒙古自治区北东部聚煤规律浅析[J].煤报.2007,98(16):60-61
    [22]刘学锋,孟令奎.松辽盆地北部深层构造的平衡剖面研究[J].西安石油大学学报.2004,4(34):503-509
    [23]侯贵廷,钱祥麟,宋新民.渤海湾盆地形成机制研究[J].北京大学学报.1998,29(5):84-88
    [24]朱春俊,王延斌.鄂尔多斯盆地东北部上古生界煤系地层成煤特征分析[J].西安科技大学学报.2010,6(30):687-730
    [25]陈冰凌,李新安,徐勤.鄂尔多斯盆地韦州煤田构造特征与控煤作用分析[J].中国煤炭地质.2009,11(21):7-11
    [26]王钟堂.中国各地区晚三叠世含煤盆地分类及其地质特征[J].中国煤田地质.1997,9(1):3-7
    [27]黄文辉,敖卫华,翁成敏等.鄂尔多斯盆地侏罗纪煤的煤岩特征及成因分析[J].现代地质.2010,6(24):1186-1197
    [28]李增学,李江涛,韩美莲,等.鄂尔多斯盆地中生界聚煤规律及对多能源共存富集的贡献[J].山东科技大学学报.2006,2(25):1-5
    [29]徐汉林,赵宗举,杨以宁,等.南华北盆地构造格局及构造样式[J].地球学报.2003,1(24):27-33
    [30]邵龙义,肖正辉,何志平等.晋东南沁水盆地石炭二叠纪含煤岩系古地理及聚煤作用研究[J].古地理学报.2006,1(8):43-52
    [31]承金,汪新文,王小牛.山西沁水盆地热史演化特征[J].现代地质.2009,6(23):1093-1099
    [32]王国力,蔡立国,汪集,等.楚雄盆地构造-热演化与古地温场研究[J].石油试验地质.20051(27):28-38
    [33]尹福光,万方,许效松,等.楚雄盆地晚三叠世古地理变迁[J].沉积与特提斯地质.2004,3(24):52-57
    [34]高彩霞,邵龙义,李长林等.四川盆地东部上三叠统须家河组层序地层及聚煤特征研究[J].古地理学报.2009,6(11):689-696
    [35]许福美,黄文辉,吴传始,等.福建龙永煤田顶峰山井田童子岩组沉积环境及演化[J].地质科学.2010,1:324-332
    [36]杨永毅,郭昆林.滇东煤田长坡井田晚二叠世聚煤环境与成煤模式[J].昆明冶金高等专科学校学报.2006,3(22):40-43
    [37]闫庆磊,朱炎铭,袁伟等.开平煤田构造发育规律对煤层赋存的影响[J].中国煤炭地质.2009,12(21):38-41
    [38]邹文康.龙永煤田罗山区构造机制及其控煤规律[J].中国煤田地质.2002,3(14):7-9
    [39]和中铧,刘招君,郭巍等.柴达木北缘中生代盆地的成因类型及构造沉积演化[J].吉林大学学报.2002,4(32):333-339
    [40]占文锋,林亮,孙红波等.柴北缘含煤区构造演化与构造控煤作用[J].中国煤炭地质.2008,10(20):25-33
    [41]曹代勇,占文锋,刘天绩等.柴达木盆地北缘构造分区与煤系赋存特征[J].大地构造与成矿学.2007,3(31):322-327.
    [42]XuWJ,Chen W G. Application of grey clustering method in eutrophication assessmentfor lake water[J]Journal of Shandong Jianzhu University,2007,22(1):49-56.
    [43]任纪舜,姜春发,张正坤,等.中国大地构造及其演化[M].北京:科学出版社,1980.
    [44]贾承造,李本亮,张兴阳.中国海相盆地的形成与演化[J].科学通报.2007.52(增刊I):1-8.
    [45]程裕淇,沈永和,张良臣.中国大陆的地质构造演化[J].中国区域地质.1995.4:289-294.
    [46]曹代勇,景玉龙,邱广忠,等.中国的含煤岩系变形分区[J].煤炭学报.1998,23(5):449-454
    [47]胡军,郑宝山,王明仕,等.中国煤中硫的分布特征及成因[J].煤炭转化.2005,28(4):1-6.
    [48]王明仕,郑宝山,胡军,等.我国煤种砷含量及分布[J].煤炭学报.2005,30(3):344-348
    [49]白向飞,李文华,陈文敏.中国煤种铍的分布赋存特征研究[J].燃料化学学报.2004,32(2):156-159
    [50]李祖材,黄宪.中国煤系构造类型的划分[J].科学通报.1980,14:875-877
    [51]罗庆银,张晓坤.中国聚煤盆地演化特征[J].科技信息.2009,21:45-46
    [52]吴根耀,梁江平,杨建国.白垩纪北东向构造与松辽盆地演化和油气成藏[J].大庆石油地质与开发.2009,28(6):1-11
    [53]王双明.鄂尔多斯盆地构造演化和构造控煤作用[J].地质通报.2011,30(4):544-552.
    [54]陈全红,李文厚,郭艳琴,等.鄂尔多斯盆地早二叠世聚煤环境与成煤模式分析[J].2009,27(1):70-76.
    [55]王双明,张玉平.鄂尔多斯侏罗纪盆地形成演化和聚煤规律[J].地学前缘.1999,6(增刊):147-154.
    [56]徐振永,王延斌,陈德元,等.沁水盆地晚古生代煤系层序地层及岩相古地理研究[J].煤田地质与勘探.2007,35(4):5-11.
    [57]曹德斌,张志斌.楚雄盆地中-新生界构造变形特征[J].云南地质.2001,21(1):50-59.
    [58]杨克绳.塔里木盆地的构造演化[J].海洋地质动态.2005,21(2):25-29
    [59]唐良杰.塔里木盆地构造演化与构造样式[J].地球科学-中国地质大学学报.1994,19(6):742-753.
    [60]吴涛,张世焕,王武和.吐哈盆地构造演化与煤成烃富集规律[J].地质论评.1996,42(增刊):31-36.
    [71]陈建军,刘池阳,姚亚明,等.中生代焉耆盆地演化特征[J].西北大学学报.2007,37(2):287-290.
    [72]叶贵钧.西北五省(区)的煤炭资源、水资源及生态环境[J].煤田地质与勘探.2000,28(6):39-42.
    [73]刘向阳,李进军,王贝.宁东煤田马家滩矿区沉积环境与聚煤作用[J].中国煤炭地质.2009,21(11):19-27.
    [74]张国伟,孟庆任,于在平,等.秦岭造山带的造山过程及其动力学特征[J].中国科学.1996,26(3):193-200
    [75]李双林,欧阳自远.兴蒙造山带及邻区的构造格局与构造演化[J].海洋地质与第四纪地质.1998,18(3):45-54
    [76]武红岭,董树文.大别造山带构造超压形成的碰撞力学机理[J].地球科学进展.2001,16(4):478-483.
    [77]丘元禧,张渝昌,马文璞.雪峰山陆内造山带的构造特征与演化[J].高校地质学报.1998,4(4):432-442.
    [78]郭斌.龙门山造山带构造特征及演化过程研究[D].中国地质大学(北京).2006
    [79]李锦轶,王克卓,李亚萍,等.天山山脉地貌特征、地壳组成与地质演化[J].地质通报.2006,25(8):895-909
    [70]柴杨.基于多条件约束的煤炭资源有效供给能力研究[D].中国矿业大学(北京).2010.
    [71]蔡东升,卢华复,贾东,等.南天山古生代板块构造演化[J].地质论评.1995,41(5):432-443
    [72]李曰俊,杨海军,赵岩,等.南天山区域打的构造与演化[J].大地构造与成矿学.2009,33(1):94-104
    [73]郝杰,刘小汉.南天山蛇绿混杂岩形成时代及大地构造意义[J].地质科学.1993,28(1):93-95
    [74]肖龙.新疆天山造山带地质构造研究进展-兼论陆间型造山带形成的五阶段模式[J].桂林工学院学报.1999,19(4):315-320
    [76]任战利,肖晖,刘丽.沁水盆地中生代构造热事件发生时期的确定[J].石油勘探与开发.2005,32(1):43-47
    [77]承金,汪新文,王小牛.山西沁水盆地热史演化特征[J].现代地质.2009,23(6):1093-1099
    [78]王国力,蔡立国,汪集.楚雄盆地构造-热演化与古地温场研究[J].石油实验地质.2005,27(1):28-38
    [79]煤炭部地质勘探研究所地质室.我国南方若干构造型式与煤田分布[J].37-42
    [80]庚立权.略论甘肃中部主要构造带与煤田分布问题[J].16-22
    [81]刘志逊,陈河替,黄文辉.我国煤炭资源现状及勘查战略[J].煤炭技术,2005,24(10):1-2
    [82]王新民,王玉怀.我国煤炭资源开发现状及存在主要问题的分析[J].华北矿业高等专科学校学报,2000,2(3):34-36.
    [83]张瑞胜.浅谈我国煤炭资源的利用现状[J].科技风,2011,254-255.
    [84]易同生.贵州省煤炭资源勘查与开发的现状、问题与对策[J].中国煤炭,2010,36(6):32-36.
    [85]薛庆远.我国煤炭资源现状及其合理开发利用[J].煤田地质与勘探,1996,24(6):23-26.
    [86]杨森从.河北省煤炭资源勘查及开发现状[J].中国煤田地质,2006,18(4):5-10.
    [87]毛德荣,侯振才.全国煤炭资源开发利用现状与保护对策的探讨[J].中国地质,1997,14-17.
    [88]吴景龙.内蒙古煤炭资源开发利用现状及对策研究[J].煤炭工程,2008,(2):101-102.
    [89]王俊民.新疆煤炭资源勘查开发现状与可持续发展[J].中国煤田地质,2001,13(3):20-21.
    [90]邱增国,孟云平,廖家隆,等.江苏省煤炭资源保障程度及勘查研究[J].中国煤炭地质,2011,23(10):75-76
    [91]唐卫国,蒋星祥,汤亚平.湖南煤炭资源开发利用现状与对策[J].中国矿业,2012,21(1):44-47.
    [92]蔡宝森,刘章现.平顶山市煤炭资源开发利用现状与发展对策[J].中国资源综合利用,2001,33-34.
    [93]田山岗,尚冠雄,唐辛.中国煤炭资源的井字型分区格局-地域分异性与资源经济地理区划[J].中国煤炭地质,2006,18(3):1-5.
    [94]程爱国,宁树正,袁同兴.中国煤炭资源综合区划研究[J].中国煤炭地质,2011,23(8):5-8.
    [95]毛节华,等.中国煤炭资源预测与评价[M].北京:科学出版社,1999.
    [96]魏同,等.中国煤炭开发战略研究[M].太原:山西科学技术出版社,1995.
    [97]刘勇.区域经济发展与地区主导产业[M].北京:商务出版社,2006.
    [101]中国能源研究会,国家电力公司战略研究与规划部.中国能源五十年[M].北京:中国电力出版社,2002.
    [102]汪应宏,郭达志,等.我国煤炭资源势的空间分布及其应用[J].自然资源学报,2006,21(2):225-231.
    [103]蔡国田,张雷.中国能源保障基本形势分析[J].地理科学进展,2006,25(5):57-67.
    [104]熊文,吴玉鸣.中国经济增长与环境脆弱性的因果及冲击响应分析[J].资源科学,2006,28(5),17-24.
    [105]刘海滨,王立杰.我国煤炭资源综合开发布局与模式研究[J].自然资源学报,2004,19(3):401-408.
    [106]魏同,张先尘,王玉浚,等.中国煤炭开发战略研究[M].太原:山西科学技术出版社,1995.
    [107]谢高地,甄霖,鲁春霞,等.中国发展的可持续性状态与趋势[J].资源科学,2008,30(9):1349~1356.
    [108]杜贵成,王永玲.我国煤炭资源中长期需求预测[J].东北财经大学学报,2007,(2):67~71.
    [109]毛节华.关于煤炭资源分类分级问题.中国煤田地质,1996;8(3):2-7.
    [110]许惠龙等.中国煤炭资源综合评价的思路和方法;.煤田地质与勘探,1997;25(1):25-28.
    [111]马蓓蓓,鲁春霞,张雷.中国煤炭资源开发的潜力评价与开发战略2009,31(2):224-230.
    [112]张雷,中国矿产资源开发与区域发展[M].北京:海洋出版社,1997.
    [112]孙立平,杜永武.煤炭资源开发与经济可持续发展[N].中国经济时报,2005-09-20.
    [114]魏振宽,荆全忠,米超.从可持续发展战略出发制定我国的煤炭资源政策[R].煤炭经济研究,2003,(7).
    [115]毛节华,许惠龙.中国煤炭资源分布现状和远景预测[J].煤田地质与勘探,1999,27(3):1-4.
    [116]中国煤田地质总局(毛节华、许惠龙主编).中国煤炭资源预测与评价[M].北京:科学出版社,1999.
    [117]徐勇.浅论矿集区的资源潜力与勘查评价,中国地质,2002,30(3):263-270.
    [118]倪斌.中国煤炭资源及其对优化能源结构的基础性作用[J].中国煤田地质,2003,15(6):3-6.
    [119]张世奎.中国煤炭资源保障程度与合理开发利用[J].中国煤田地质,2004,16(1):1-3.
    [120]王永,王咚,康高峰等.中国可供性煤炭资源潜力分析(J).中国地质,2009,36(6):845-852.
    [121]程爱国,曹代勇,袁同星.全国煤炭资源潜力评价技术要求[M].北京:地质出版社,2010.
    [122]李军.中国洁净煤技术出口的战略选择[J].中国煤炭1998(1).
    [123]唐书恒,李正越.试论有序开发西部优质煤炭资源[J].中国煤田地质,2001,13(2):105-106.
    [124]李小彦,晋香兰,李贵红.西部煤炭资源开发中优质煤概念及利用问题的思考[J].中国煤田地质,2005,17(3):5-8.
    [125]骆振福.中国西部煤炭能源的优化利用[J].中国矿业,2001,10(1):36-39.
    [126]曹代勇,赵锋华.重视我国优质煤炭资源特性的研究[J].中国矿业,2003,12(10):21-23.
    [127]李小彦,王杰玲,赵平.鄂尔多斯盆地优质煤的分类与评价[J].煤田地质与勘探,2007,35(4):1-4.
    [128]国土资源部矿产资源储量司编.2003.固体矿产地质勘查规范的新变革.北京:地质出版社.
    [129]田山岗等.2001.中国煤炭资源有效供给能力态势分析.中国煤田地质(增刊).
    [130]国土资源部矿产资源储量评审中心编.2005.固体矿产资源储量分类概论.北京:中国文联出版社.
    [131]田山岗,尚冠雄等.煤炭资源评价探析,1999,山西科学技术出版社.
    [132]《专家:能源紧缺更要摸清家底加强管理》,新华网,2004-04-04.
    [133]曾勇.中国西部地区特殊煤种及其综合开发与利用[J].煤炭学报,2001,26(4),337-340.
    [134]金世雄,姜瑗,蔡乃仲等.中国煤炭资源形势分析及合理开发利用[M]北京:地质出版社,1997.
    [135]高洪烈.煤炭的资源储备和安全供应问题讨论[J].中国煤田地质,2001(4).
    [136]胡崇梅.论煤炭资源的战略储备[J].山西焦煤科技,2008(5).
    [137]吕涛,聂锐.浅析煤炭应急供应保障体系建设-以江苏省为例[J].煤炭经济研究,2008(12).
    [138]李金克.我国煤炭战略储备研究[J].煤炭经济研究,2009(10).
    [139]孙升林,王玉林.我国东部煤炭资源状况及勘查前景浅析[J].煤炭经济研究,2008(7):4-6.
    [140]付兴方,焦颖.浅析我国稀缺品种煤炭资源的可持续利用[J].地质技术经济管理,1999,21(5-6):103-107.
    [141]马庆元.中国炼焦煤资源分布特征[J].煤炭科学技术,2004,32(3):63-66.
    [142]樊永山,石耀祥,潘莹,等.我国炼焦煤资源的合理开发与保护[J].山西焦煤科技,2008,(3):1-3.
    [143]叶大武.我国焦煤产业现状及其对策建议[J].中国煤炭,2005,31(2):49-51.
    [144]陈武,李云峰.我国能源可持续发展的探讨[J].能源技术经济,2010,22(5):17-23.
    [145]倪斌.中国的煤炭资源及其对优化能源结构的基础性作用,中国煤炭地质,2003,15(6)3-7.
    [149]汪云甲,黄宗文.矿产资源评价及其应用研究「M].徐州:中国矿业大学出版社,1998年.
    [150]王俊庸.适于综采的地质条件评价方法简介「J}.煤矿设计,1988,(11):17-23.
    [151]中国煤炭工业百科全书编辑委员会.中国煤炭工业b科全}洲地质、到量卷)[M].北京:煤炭工业出版社,1996.
    [152]曹代勇,邵龙义,张鹏飞.吐哈盆地早、中侏罗世聚煤期古构造[J].古地理学报.1999,1(2):46-51
    [153] R. Meij and H. Winkel: The emissions of heavy metals and persistent organic pollutants from moderncoal-fired power stations. Atmos. Environ. Vo1.41(2007), p.9262-9272
    [154] Y Zhao, S.X. Wang, C.P. Nielsen, X.H. Li and J.M. Hao: Establishment of a database of emissionfactors for atmospheric pollutants from Chinese coal-fired power plants. Atmos. Environ. Vo1.44{2010),p.1515-1523.
    [155]Y Zhao, S.X. Wang, L. Duan, Y Lei, P.F. Cao and J.M. Hao: Primary air pollutant emissions ofcoal-fired power plants in China: Current status and future prediction. Atmos. Environ. Vo1.42(2008),p.8442-8452.
    [156] Gregory Mankiw. Principles of Economics[M]. Parragon.U.S.2007.
    [157] ZHANG Ying, WANG Huan-chen.Development and application of P-S aided decisionsystem[J].Systems Engineering-Theory Methodology Applications,2002,11(4):324-329.
    [158]Steve Fiscor. Coal cperators invest in longwall technology[J].Coal Age,2002,17(2):28-32.
    [159]Stern D. The rise and fall of the environmental Kmnets curve.World Development,2004.(8):1419-1439.
    [160]XIE Gaodi,ZHEN Lin,LU Chunxia,et al. Sustainability status and trends of China s development:An assessment based on the natural resource base [J].Resources Science,2008,30(9):1349~1356.
    [162] North American Geologic Map Data Model Steering Committee Data Model Design Team.NADMConceptual Model1,0-A Conceptual Model for Geologic Map Information[M].United States: U.S.Department of the Interior&U.S. Geological Survey,2006:6-48.
    [161] K. Soucek} L. Stash R. Snuparek. Laboratory research of coal geocomposits PROCEEDINGS OFXII INTERNATIONAL CONGRESS OF INTERNATIONAL SOCIETY FOR M INE SURVEYING2004SEP.
    [162]Dai S F, Chou C L, Yue M, et al M ineralogy and geochem is-try of a late Pem} ian coalin the Dafang Coalfield G u izh ou,China influence from siliceous and iron-rich calcichydrothermal fluids[J]. International Journal of Coal Geology,2005(3-4).
    [163] LIU Haibin,WANG Lijie.Study on integrated development layout and mode of coal resources inChina[J]. Journal of Natural Resources,2004,19(3):401~408.
    [166] XIONG Wen,WUYuming. Causality and impulse response on the relationship of China s economicgrowth and environment fragility[J].Resources Science,2006,28(5):17~24.
    [164]CAI Guotian,ZHANG Lei. Analysis basic situation of China s energy security[J]. Process inGeography,2006,25(5):57~67.
    [165] WANG Yinghong,GUO Dazhi,ZHANG Hairong,et al. Spatial distribution and applications of coalresource potential in China[J]. Journal of Natural Resources,2006,21(2):225~231.
    [166]Committee of Chinese Energy Research,Strategy and Planning Research Department of NationalPower Company. Chinese Energy50Years[M].Beijing: Chinese Electric Power Publishing House,2002.237~360.
    [167]ZHANG Lei. The Mine Resources Exploration and National Industrialization[M]. Beijing:Commercial Press,2004.
    [168]DU Guicheng,WANG Yongling.The middle and long-term predict of coal resources inChina[J].Journal of Northeast Finance and Economics University,2007,(2):67~71.
    [169] Hongzhu Song,Suizheng Wang.Applications of3D stratum isualization CAD in GeologicalExploration. Advanced Materials Research Vols.798-799(2013) pp369-373.
    [170] Sedimentary facies and coal-accumulation of Early-Middle Jurassic in Toksun coalfield NorthwesternChina. ENERGY EXPLORATION&EXPLOITATION2013,31(2):459~470.
    [171] Grey-Risk Estimation of the Water Inrush from No.9Coal Floor in Guoerzhuang Mine. AppliedMechanics and Materials Vols.295-298(2013) pp3019-3022.
    [172] Peter Nolan. China and the Global Economy:national champi ons,industrial policy,and the bigbusiness revolution [M].Houndmills,Basingstoke,Hampshire;New York Palgrave,2001.
    [173] Larsona E D,Wu Z,Delaquil P.Future implications of China s energy-technology choices[J]. EncrgyPolicy,2003,31:1189-1204.
    [174] LIU H, Huang H, The Calculating Model for Development Investment of Coal Resources Based onANN. In5th International Symposium on Mining Science and Technology, XU Zhou,2004.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700